Climate Dynamics

, Volume 50, Issue 9–10, pp 3849–3851 | Cite as

Correction to: Emergence of deep convection in the Arctic Ocean under a warming climate

  • Camille Lique
  • Helen L. Johnson
  • Yves Plancherel
Correction

1 Correction to: Clim Dyn  https://doi.org/10.1007/s00382-017-3849-9

In the original article, Figures 3, 4 and 5 are the same one (a duplication of Figure 4).

The corrected version of Figures 3 and 5 is given below. The original article was corrected.
Fig. 3

Mean March and September sea surface temperature (SST, in \(^{\circ }\)C) for the CTRL and the \(4 \times \text {CO}_2\) runs and the difference between the two runs. For the bottom raw, black hatching indicates areas where the difference between the two runs is not significant. The red contour corresponds to the location of the sea ice edge (defined as the 15% concentration contour), and the black contour on the bottom panels shows the 500 m isobath

Fig. 5

Mean March and September sea surface potential density (\(\sigma \), in \(\text {kg/m}^3\)) for the CTRL and the \(4 \times \text {CO}_2\) runs and the difference between the two runs. For the bottom raw, black hatching indicates areas where the difference between the two runs is not significant. The red contour corresponds to the location of the sea ice edge (defined as the 15% concentration contour), and the black contour on the bottom panels shows the 500 m isobath

Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2017

Authors and Affiliations

  1. 1.Laboratoire d’Océanographie Physique et Spatiale, UMR6523, CNRS-Ifremer-UBO-IRDBrestFrance
  2. 2.Department of Earth SciencesUniversity of OxfordOxfordUK

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